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Flood Assessment

Climate Change and Flood Design in New Zealand: HIRDS, RCP 6.0, RCP 8.5, and What They Mean for Your Site

New Zealand flood design now requires climate change uplift, but how much uplift, and which RCP scenario to apply, depends on your council, your catchment, and your intended design life. HIRDS (High Intensity Rainfall Design System) provides the rainfall frequency data, but converting that to a flood peak requires knowing which return period to combine with which RCP pathway. Getting this wrong means either an under-designed structure or an over-engineered one, and councils are increasingly scrutinising the methodology.

What HIRDS provides

HIRDS is NIWA's online tool for estimating rainfall intensity at any location in New Zealand for a range of return periods (2-year to 100-year and beyond) and storm durations (10 minutes to 72 hours). It draws on the national rainfall gauge network and provides depth-duration-frequency (DDF) tables that form the basis of most flood design in the country.

Critically, HIRDS v4 includes climate change uplift factors for four RCP scenarios (2.6, 4.5, 6.0, and 8.5) at two future time horizons (2031-2050 and 2081-2100). These factors increase the historical rainfall intensities by a percentage that reflects projected changes in atmospheric moisture under each emissions pathway.

What the RCP scenarios mean in practice

RCP stands for Representative Concentration Pathway. The number after "RCP" represents the radiative forcing in watts per square metre by the year 2100. In practical terms for flood design:

The difference between RCP 6.0 and RCP 8.5 can translate to a 10 to 15% increase in the design flood peak. On a flat floodplain, that can mean 200 to 400 mm of additional flood depth at a building platform.

Which RCP do councils require?

This is where practice varies significantly across New Zealand. Some councils have clear policy; others leave it to the engineer's professional judgement.

MfE (Ministry for the Environment) guidance recommends using RCP 8.5 for infrastructure with a design life beyond 2100, and at least RCP 6.0 for shorter-lived assets. In practice, most regional councils now expect RCP 8.5 at the 2081-2100 horizon for residential subdivision consent applications, on the basis that houses built today will still be occupied in 75 years.

On the Tukituki River flood study, RCP 8.5 at the 2081-2100 horizon was adopted for the primary flood hazard assessment. RCP 6.0 was also run for comparison, producing a Q100 approximately 12% lower.

How climate change uplift flows through the design

The uplift factor applies to the rainfall input, not directly to the flood flow output. The relationship between increased rainfall and increased flood peak is not one-to-one, because the catchment's losses (infiltration, initial abstraction) absorb some of the additional rainfall before it becomes runoff.

For a catchment with high CN (mostly impervious or saturated soils), a 20% increase in rainfall might produce a 22 to 25% increase in peak flow. For a more permeable catchment with lower CN, the same 20% rainfall increase might only produce a 15 to 18% increase in peak flow. This is why the SCS loss model and the climate change scenario need to be considered together, not independently.

Practical recommendations

For developers and landowners commissioning flood studies:

Key takeaway

Climate change uplift is now a standard requirement for NZ flood design. HIRDS provides the uplift factors, but the choice of RCP scenario (usually RCP 8.5 for residential) and time horizon directly affects flood levels and building platform requirements. Confirm your council's expectations before commissioning the study.

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Andre Magdich
CPEng - Director, SAE Ltd

Andre is a Chartered Professional Engineer with 15+ years of civil engineering experience and 300+ completed projects across New Zealand. SAE Ltd specialises in stormwater design, flood hazard assessment, and subdivision infrastructure. Based in Napier, Hawke's Bay.

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